<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Yoshida K</submitter><funding>Japan Society for the Promotion of Science</funding><pagination>7117</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC10170078</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>13(1)</volume><pubmed_abstract>Nanometer-sized crystals (nanolites) play an important role in controlling eruptions by affecting the viscosity of magmas and inducing bubble nucleation. We present detailed microscopic and nanoscopic petrographic analyses of nanolite-bearing and nanolite-free pumice from the 2021 eruption of Fukutoku-Oka-no-Ba, Japan. The nanolite mineral assemblage includes biotite, which is absent from the phenocryst mineral assemblage, and magnetite and clinopyroxene, which are observed as phenocrysts. The boundary between the nanolite-bearing brown glass and nanolite-free colorless glass is either sharp or gradational, and the sharp boundaries also appear sharp under the transmitted electron microscope. X-ray absorption fine structure (XAFS) analysis of the volcanic glass revealed that the nanolite-fr</pubmed_abstract><journal>Scientific reports</journal><pubmed_title>Oxidation-induced nanolite crystallization triggered the 2021 eruption of Fukutoku-Oka-no-Ba, Japan.</pubmed_title><pmcid>PMC10170078</pmcid><funding_grant_id>JP20H00198</funding_grant_id><funding_grant_id>JP21H01195</funding_grant_id><funding_grant_id>JP20H00205</funding_grant_id><funding_grant_id>JP22K03755</funding_grant_id><funding_grant_id>JP18KK0376</funding_grant_id><funding_grant_id>JP22H05109</funding_grant_id><funding_grant_id>JP19K14825</funding_grant_id><funding_grant_id>JP19H01999</funding_grant_id><funding_grant_id>JP19H00834</funding_grant_id><pubmed_authors>Sato T</pubmed_authors><pubmed_authors>Miyake A</pubmed_authors><pubmed_authors>Niwa Y</pubmed_authors><pubmed_authors>Okumura S</pubmed_authors><pubmed_authors>Okamoto A</pubmed_authors><pubmed_authors>Tamura Y</pubmed_authors><pubmed_authors>Ishibashi H</pubmed_authors><pubmed_authors>Okumura SH</pubmed_authors><pubmed_authors>Yoshida K</pubmed_authors><pubmed_authors>Kimura M</pubmed_authors><pubmed_authors>Ono S</pubmed_authors></additional><is_claimable>false</is_claimable><name>Oxidation-induced nanolite crystallization triggered the 2021 eruption of Fukutoku-Oka-no-Ba, Japan.</name><description>Nanometer-sized crystals (nanolites) play an important role in controlling eruptions by affecting the viscosity of magmas and inducing bubble nucleation. We present detailed microscopic and nanoscopic petrographic analyses of nanolite-bearing and nanolite-free pumice from the 2021 eruption of Fukutoku-Oka-no-Ba, Japan. The nanolite mineral assemblage includes biotite, which is absent from the phenocryst mineral assemblage, and magnetite and clinopyroxene, which are observed as phenocrysts. The boundary between the nanolite-bearing brown glass and nanolite-free colorless glass is either sharp or gradational, and the sharp boundaries also appear sharp under the transmitted electron microscope. X-ray absorption fine structure (XAFS) analysis of the volcanic glass revealed that the nanolite-fr</description><dates><release>2023-01-01T00:00:00Z</release><publication>2023 May</publication><modification>2025-04-05T10:55:04.764Z</modification><creation>2025-04-05T10:55:04.764Z</creation></dates><accession>S-EPMC10170078</accession><cross_references><pubmed>37160932</pubmed><doi>10.1038/s41598-023-34301-w</doi></cross_references></HashMap>